Search results for "Vial"

showing 10 items of 408 documents

Red fluvial y niveles de terrazas en la depresión Cocentaina-Muro (Valls d'Alcoi)

1975

UNESCO::HISTORIAGeografíaUNESCO::HISTORIA::Historia por épocas::Historia antiguaRed fluvial y niveles de terrazas en la depresión Cocentaina-Muro (Valls d'Alcoi) ArtículoHumanidadesGeociencias. Medio ambienteGrupo BGrupo C:HISTORIA [UNESCO]:HISTORIA::Historia por épocas::Historia antigua [UNESCO]Historia
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Los depósitos cuaternarios de L'Arenal de Petrer (Alicante)

1988

EN ESTE ARTICULO SE ESTUDIA LA GEOMORFOLOGIA Y LOS DEPOSITOS CUATERNARIOS DE UNA PEQUEÑA RAMBLA DE LA PROVINCIA DE ALICANTE, TRIBUTARIA DEL VINALOPO. DESDE LA PERSPECTIVA ESTRATIGRAFICA Y SEDIMENTOLOGICA, APOYADOS EN DATACIONES ABSOLUTAS DE C14 SE HA INTENTADO ESTABLECER LA SECUENCIA SEDIMENTARIA, QUE REFLEJA EL COMPORTAMIENTO DEL VALLE DURANTE LAS ULTIMAS PULSACIONES CLIMATICAS CUATERNARIAS. (A)

UNESCO::HISTORIAGeografíaUNESCO::HISTORIA::Historia por épocas::Historia antiguaTaffoniSedimentos eólicosGeociencias. Medio ambienteEstratigrafíaModelado:HISTORIA::Historia por épocas::Historia antigua [UNESCO]Depósitos aluvialesCuencas fluvialesMedio físicoGrupo BRedes de drenajeMantos coluviales:HISTORIA [UNESCO]CuaternarioOscilaciones climáticasCarbono 14
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Attitude and speed in young people. Implementation of a program of driver education

2009

Contemporary Theories of change of attitudes defends that these depends on the way to think, to act and to feel of the people. If we touch upon each one of these three main components related between we can influence in the predisposition to act. The application of a program of speed self-control to ample of young drivers, using a design pretest- postest with control group and using a Factor Analysis shows that is possible the change of attitudes.

VelocidadCambio de actitudes; Velocidad; Investigación en educación y seguridad vial; Educación y formación viales; Seguridad vialCambio de actitudesInvestigación en educación y seguridad vialSeguridad vialEducación y formación viales
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Travelling Strings, Beams, Panels, Membranes and Plates

2013

In this chapter, we will introduce in a general manner some of the most common models for axially travelling materials, which will be used in the rest of the book. We will introduce the linear models of travelling strings, panels, and plates. It will be assumed that the material is thin, i.e. its planar dimensions are much larger than its thickness. We will work in the small displacement regime, that is, with linear models approximating the behaviour of the system near the trivial equilibrium. As is well known in the theory of elasticity, this approximation allows for a decoupling of the in-plane and out-of-plane components in the dynamics of the system. We will concentrate on small out-of-…

VibrationPhysicsTransverse planeClassical mechanicsPlanarTrivial equilibriumLinear modelFlexural rigidityDecoupling (cosmology)Axial symmetry
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Miocene to recent history of the western Altiplano in northern Chile revealed by lacustrine sediments of the Lauca basin (18�15??18�40? S/69�30??69�0…

1995

The intramontane Lauca Basin at the western margin of the northern Chilean Altiplano lies to the west of and is topographically isolated from the well-known Plio-Pleistocene lake system of fluvio-lacustrine origin that covers the Bolivian Altiplano from Lake Titicaca to the north for more than 800 km to the Salar de Uyuni in the south. The Lauca Basin is filled by a sequence of some 120 m of mainly upper Miocene to Pliocene elastic and volcaniclastic sediments of lacustrine and alluvial origin. Volcanic rocks, partly pyroelastic, provide useful marker horizons. In the first period (6–4 Ma) of its evolution, the ‘Lago Lauca’ was a shallow ephemeral lake. Evaporites indicate temporarily close…

Volcanic rockgeographyPaleontologygeography.geographical_feature_categoryPleistoceneEvaporiteGeneral Earth and Planetary SciencesAlluviumStructural basinSedimentologyHoloceneGeologyAlluvial plainGeologische Rundschau
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Structure of longitudinal chromomagnetic fields in high energy collisions

2014

We compute expectation values of spatial Wilson loops in the forward light cone of high-energy collisions. We consider ensembles of gauge field configurations generated from a classical Gaussian effective action as well as solutions of high-energy renormalization group evolution with fixed and running coupling. The initial fields correspond to a color field condensate exhibiting domain-like structure over distance scales of order the saturation scale. At later times universal scaling emerges at large distances for all ensembles, with a nontrivial critical exponent. Finally, we compare the results for the Wilson loop to the two-point correlator of magnetic fields.

We compute expectation values of spatial Wilson loops in the forward light cone of high-energy collisions. We consider ensembles of gauge field configurations generated from a classical Gaussian effective action as well as solutions of high-energy renormalization group evolution with fixed and running coupling. The initial like structure over distance scales of oder the saturation scale. At later times universal scaling emerges at large distances for all ensembles with a nontrivial critical exponent. Finally we compare the resulats for the Wilson loop to the two-point correlator of magnetic fields. (C) 2014 The Authors. Published by Elsevier BV This is an open access article under the CC BY licenseNuclear and High Energy PhysicsWilson loopLARGE NUCLEINuclear TheoryField (physics)FOS: Physical sciences114 Physical sciences01 natural sciencesColor-glass condensateRENORMALIZATION-GROUPNuclear Theory (nucl-th)GLUON DISTRIBUTION-FUNCTIONSHigh Energy Physics - Phenomenology (hep-ph)Light cone0103 physical sciencesSCATTERINGGauge theory010306 general physicsSMALL-XEffective actionPhysicsCORRELATORSta114010308 nuclear & particles physicsCOLOR GLASS CONDENSATERenormalization groupEVOLUTIONJIMWLK EQUATIONHigh Energy Physics - PhenomenologySATURATIONQuantum electrodynamicsCritical exponentPhysics Letters B
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Generalized fuzzy topology versus non-commutative topology

2011

The paper introduces a modification of the notions of generalized fuzzy topological space of Demirci and quantal space of Mulvey and Pelletier, suitable to explore interrelations between point-set lattice-theoretic topology and non-commutative topology developed in the framework of C^*-algebras or (more recently) of quantales. As a consequence of the new approach, a generalization of the concept of topological system of Vickers arises. Moreover, the currently dominating variable-basis topological setting in the fuzzy community, due to Rodabaugh, appears to be ''fixed-basis''.

Weak topologyArtificial IntelligenceLogicTrivial topologyExtension topologyProduct topologyInitial topologyGeneral topologyParticular point topologyTopological spaceTopologyMathematicsFuzzy Sets and Systems
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El contacte entre la Ribera del Xúquer i els raiguers de les Muntanyes de Carcaixent

1985

Cuando el río Xúquer llega a la Ribera, deja el encajamiento montañoso y forma un cono aluvial que ent ra en contacto con los piedemontes originados por los relieves emergidos en las cercanías de la llanura de inundación, apareciendo unas zonas deprimidas en el punto de contacto de las dos formaciones por los perfiles opuestos que presentan. Además, el contacto no es estable debido a la diferente velocidad de crecimiento en altura, y en consecuencia los depósitos fluviales conquistan poco a poco las tierras de piedemonte y por lo tanto, la zona deprimida se aleja cada vez más del río. En segundo lugar, los núcleos de población, que hace muchos años estaban al margen de las inundaciones por …

Zonas de contactoUNESCO::HISTORIAGeografíaUNESCO::HISTORIA::Historia por épocas::Historia antiguaAsentamientosGeociencias. Medio ambienteFactores climáticos:HISTORIA::Historia por épocas::Historia antigua [UNESCO]Depósitos aluvialesMorfología fluvialGrupo B:HISTORIA [UNESCO]Llanuras de inundaciónGlacis de erosión
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Hydrogéomorphologie du site, paléoenvironnements et dynamique alluviale.

2015

In Landuré C., Arcelin P., Arnaud-Fassetta G. (Eds.) Le village de La Capelière en Camargue (Arles, Bouches-du-Rhône) du début du Ve s. av. n. è. à la période du Haut Moyen Âge - 2017

[ SDU.STU.GM ] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.GEO] Humanities and Social Sciences/GeographyCamargue[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SHS.GEO]Humanities and Social Sciences/Geography[SHS]Humanities and Social Sciences[SDU] Sciences of the Universe [physics]paléoenvironnementHydrogéomorphologie[SDU]Sciences of the Universe [physics][SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology[SHS] Humanities and Social SciencesFrance[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphologydynamique alluviale[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/Hydrology[ SDU ] Sciences of the Universe [physics]ComputingMilieux_MISCELLANEOUS
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On the use of geophysical methods to characterize heterogeneities of quaternary alluvial deposits. Application to stormwater infiltration.

2007

Colloque avec actes et comité de lecture. International.; International audience; Stormwater infiltration basins are generally built on geological formations with large values of hydraulic conductivity. Such is the case for quaternary alluvial formations, among which are glaciofluvial deposits. Two geophysical investigation methods, namely ground-penetrating radar and electrical tomography, were tested on an infiltration basin built on a glaciofluvial deposit. Geophysical profiles were calibrated on a trench wall dug in the glaciofluvial formation. A sedimentological study coupled to geophysical measurements behind the trench wall highlights the three-dimensional architecture of the deposit…

[SDE.IE]Environmental Sciences/Environmental Engineering[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]GPR[SDE.MCG]Environmental Sciences/Global Changes[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]infiltration[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.GP ] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph][ SDE.MCG ] Environmental Sciences/Global Changesstormwater infiltration[ PHYS.PHYS.PHYS-GEO-PH ] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environment[SDE.IE] Environmental Sciences/Environmental Engineering[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/Hydrology[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology[ SDU.STU.AG ] Sciences of the Universe [physics]/Earth Sciences/Applied geologyelectrical resistivityglaciofluvial deposit
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